Soil Data Explorer - ANGIE

Official Series Description

Lab Data Summary

Aggregate lab data for the ANGIE soil series. This aggregation is based on all pedons with a current taxon name of ANGIE, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to ANGIE were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Pedons used in the lab summary:

MLRA	Lab ID	Pedon ID	Taxonname	CI	NSSL / NASIS Reports	Link To SoilWeb GMap
133A	S57_030	1974-FL113-S57_030	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.7612896,-87.2860794
133A	S57_032	1974-FL113-S57_032	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.6571026,-87.2335968
133A	S66_022	1979-FL131-S66_022	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	30.6770992,-86.1711578
133B	68OT01	1968AR10301	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.56028,-92.94222
133B	68OT12	1968AR10312	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.55806,-92.97972
133B	71JF03	1971AR06903	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.0825,-92.0822
135B	68HW20	1968AR06120	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	34.0683,-93.8942
135B	68HW31	1968AR06131	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.8556,-93.9694
135B	68HW37	1968AR06137	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	33.8661,-93.8789
n/a	S30_004	1969-FL059-S30_004	Angie	3	Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties	n/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ANGIE soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the ANGIE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the ANGIE series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the ANGIE series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

There are insufficient data to create the 3D mountains figure.

Competing Series

Soil series competing with ANGIE share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the ANGIE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the ANGIE series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

There are insufficient data to create the 3D mountains figure.

Soil series sharing subgroup-level classification with ANGIE, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database (updated 2024-10-23).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. AL-2012-04-24-12 | Greene County - June 1971

   Cross section of association 3 showing topography, important soils, and underlying material (Soil Survey of Greene County, Alabama; June 1971).

2. FL-2012-04-26-27 | Washington County - May 1965

   Geologic formations of Washington County and the position of most soil series (Soil Survey of Washington County, Florida; May 1965).

Map Units

Map units containing ANGIE as a major component. Limited to 250 records.

Map Unit Name	Symbol	Map Unit Area (ac)	Map Unit Key	National Map Unit Symbol	Soil Survey Area	Publication Date	Map Scale
Angie-Wickham complex, 0 to 2 percent slopes	AwA	3273	328485	c0t9	al021	1967	1:20000
Angie-Wickham complex, 2 to 6 percent slopes	AwB	683	328486	c0tb	al021	1967	1:20000
Shubuta and Angie very fine sandy loams, eroded, gently sloping	ScC2	12867	329037	c1d3	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, eroded, very gently sloping	ScB2	8120	329035	c1d1	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, eroded, sloping	ScD2	7586	329039	c1d5	al045	1958	1:20000
Shubuta and Angie sandy clay loams, severely eroded, gently sloping	SbC3	2059	329033	c1cz	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, sloping	ScD	970	329038	c1d4	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, very gently sloping	ScB	766	329034	c1d0	al045	1958	1:20000
Shubuta and Angie sandy clay loams, severely eroded, very gently sloping	SbB3	584	329032	c1cy	al045	1958	1:20000
Shubuta and Angie very fine sandy loams, gently sloping	ScC	554	329036	c1d2	al045	1958	1:20000
Angie fine sandy loam, 2 to 5 percent slopes	3	4456	329066	c1f1	al047	1977	1:20000
Angie fine sandy loam, 5 to 12 percent slopes	4	3377	329077	c1fd	al047	1977	1:20000
Angie fine sandy loam, 0 to 2 percent slopes	2	2419	329055	c1dp	al047	1977	1:20000
Leaf-Angie association	LF	15739	329668	c21g	al063	2013	1:
Angie fine sandy loam, terrace, 0 to 2 percent slopes	AgA	8680	329647	c20s	al063	2013	1:
Angie-Leaf association	AS	4370	329644	c20p	al063	2013	1:
Angie fine sandy loam, 2 to 5 percent slopes	AfB	2361	329645	c20q	al063	2013	1:
Angie fine sandy loam, 5 to 8 percent slopes, eroded	AfC2	1047	329646	c20r	al063	2013	1:
Angie sandy clay loam, 5 to 12 percent slopes, severely eroded	AnD3	803	329649	c20v	al063	2013	1:
Angie fine sandy loam, terrace, 2 to 5 percent slopes	AgB	446	329648	c20t	al063	2013	1:
Angie silt loam, 0 to 1 percent slopes	AnA	1277	565288	2ykhc	ar025	1965	1:15840
Angie silt loam, 1 to 3 percent slope	AnB	446	565289	2xz2b	ar025	1965	1:15840
Angie fine sandy loam, 3 to 8 percent slopes	4	18293	565369	2xz22	ar027	1983	1:20000
Angie fine sandy loam, 1 to 3 percent slopes	3	9894	565366	lz9m	ar027	1983	1:20000
Angie silt loam, 1 to 3 percent slopes	AnB	6007	565686	lzmy	ar061	1970	1:24000
Angie silt loam, 3 to 8 percent slopes	AnC	3120	565687	lzmz	ar061	1970	1:24000
Angie fine sandy loam, 1 to 8 percent slopes	AnC	64	721485	s6rq	ar099	2000	1:24000
Angie fine sandy loam, 3 to 8 percent slopes	5	1435	566245	2xz22	ar125	1976	1:20000
Angie fine sandy loam, 1 to 8 percent slopes	AnC	713	579187	mfpg	ar139	1992	1:24000
Angie fine sandy loam	3	1420	1017236	134j2	fl059	1971	1:12000
Bonifay-Dothan-Angie complex, 5 to 12 percent slopes	49	11920	1444731	1khc7	fl091	1989	1:20000
Angie sandy loam, 2 to 5 percent slopes	35	1360	1444717	2w4g4	fl091	1989	1:20000
Angie variant loam	2	1700	823749	wn5k	fl113	1978	1:20000
Bonneau-Norfolk-Angie complex, 5 to 12 percent slopes	38	20210	324008	bw4w	fl131	1985	1:20000
Angie sandy loam, 2 to 5 percent slopes	37	1960	324007	2w4g4	fl131	1985	1:20000
Angie fine sandy loam, frequently flooded	Au	11743	125336	46f3	ga609	1967	1:20000
Angie fine sandy loam	Av	4435	326024	by7x	ga646	1971	1:20000
Angie very fine sandy loam, 1 to 3 percent slopes	AnB	4	2400534	2ynxp	la013	1992	1:24000
Angie very fine sandy loam, 1 to 3 percent slopes	An	7863	569310	2ynxp	la027	1986	1:20000
Angie very fine sandy loam, 1 to 3 percent slopes	AnB	8330	571109	2ynxp	la061	1991	1:24000
Angie very fine sandy loam, 1 to 5 percent slopes	An	5980	1725322	1vxbk	la111	1992	1:24000
Angie very fine sandy loam, 1 to 5 percent slopes	AnC	614	1725528	1vxk6	la115	1992	1:24000
Angie silt loam, 1 to 5 percent slopes	Ag	1029	1724137	1vw3b	la117	1989	1:24000
Angie fine sandy loam, 5 to 8 percent slopes, eroded	AnC2	2778	331967	c4fm	ms023	1963	1:15840
Angie fine sandy loam, 2 to 5 percent slopes	AnB	1510	331966	c4fl	ms023	1963	1:15840
Angie fine sandy loam, 0 to 2 percent slopes	AnA	271	331965	c4fk	ms023	1963	1:15840
Angie silt loam, 0 to 2 percent slopes	AnA	1184	332250	c4qr	ms039	1967	1:20000
Angie fine sandy loam, 0 to 2 percent slopes	AgA	513	2642152	2rrx9	ms041	2012	1:24000
Angie fine sandy loam, 0 to 2 percent slopes	AnA	1465	131733	4f2g	sc615	1981	1:20000
Angie fine sandy loam	An	1821	575566	m9xn	tx339	1967	1:20000
Angie loam, 0 to 2 percent slopes	AgA	3211	119192	400x	va087	1973	1:15840
Angie loam, 2 to 6 percent slopes	AgB	813	119193	400y	va087	1973	1:15840
Angie loam, 2 to 6 percent slopes, eroded	AgB2	463	119194	400z	va087	1973	1:15840
Angie loam, 6 to 10 percent slopes, eroded	AgC2	405	119195	4010	va087	1973	1:15840
Angie loam, 10 to 25 percent slopes, eroded	AgE2	234	119196	4011	va087	1973	1:15840
Angie loam, concretionary subsoil variant	Ak	217	119197	4012	va087	1973	1:15840

Map of Series Extent

Approximate geographic distribution of the ANGIE soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry (updated 2024-10-30).